The potential is related to the mass exchange, calculated from the hydraulic gradient, conductivity and the potential change per
unit change in mass.
Not exact matches
By definition, it is the only object
in existence with a
mass of exactly 1 kilogram — one of the seven SI base
units — so metrologists were unsettled to discover that this
mass had
changed.
Re 423 Chris G — whether the effect saturates at a given density depends on the way the temperature is distributed; if the temperature from TOA downward is isothermal for a sufficient thickness, than the effect could be saturated at TOA (if starting from a large enough optical thickness per
unit atmospheric
mass path, a
change in the density of the gas / etc that contributes optical thickness would then have little to no effect on the flux at TOA, which is what is meant by saturation.
About increasing optical thickness per
unit mass path (via
changes in composition or imposed conditions)--
1) Start by computing the total GHG - free air constant
mass per
unit area of a gas layer between any two heights under gravity g 2) Add
in the hydrostatic equilibrium pressure
change with height
in the gravity field 3) Compute the total enthalpy per
unit area of the layer realizing the layer possesses potential energy per
unit area
in earth's gravity field 4) From that, realize energy conservation imposes a constraint that total dry static energy is constant
in the layer (within adiabatic control volume) 5) From this, realize and compute the total entropy (S) of the layer over the height of the layer 6) Transform S computation from height to pressure by way of hydrostatic eqn.
Living tree
mass could
change because of net
changes in forested area (due to natural or human causes) or because of
changes to tree
mass per
unit area (due to increases
in density or average tree size).